Independent variations of CH4 emissions and isotopic composition over the past 160,000 years - Test2 - elhamkhani - TriplyDB

Independent variations of CH4 emissions and isotopic composition over the past 160,000 years

Independent variations of CH4 emissions and isotopic composition over the past 160,000 years

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Understanding the glacial methane cycle.Minimal geological methane emissions during the Younger Dryas-Preboreal abrupt warming event.Glacial/interglacial wetland, biomass burning, and geologic methane emissions constrained by dual stable isotopic CH4 ice core records.Automated simultaneous measurement of the δ(13) C and δ(2) H values of methane and the δ(13) C and δ(18) O values of carbon dioxide in flask air samples using a new multi cryo-trap/gas chromatography/isotope ratio mass spectrometry system.Permafrost thawing as a possible source of abrupt carbon release at the onset of the Bølling/Allerød.Fully automated, high-throughput instrumentation for measuring the δ13C value of methane and application of the instrumentation to rice paddy samples.Atmospheric methane variability: Centennial-scale signals in the Last Glacial Period Carbon isotope ratios suggest no additional methane from boreal wetlands during the rapid Greenland Interstadial 21.2

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Independent variations of CH4 emissions and isotopic composition over the past 160,000 years

http://www.wikidata.org/entity/Q58053636

description

article

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im August 2013 veröffentlichter wissenschaftlicher Artikel

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wetenschappelijk artikel

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наукова стаття, опублікована в серпні 2013

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Independent variations of CH4 ...... on over the past 160,000 years

@en

Independent variations of CH4 ...... on over the past 160,000 years

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type

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Independent variations of CH4 ...... on over the past 160,000 years

@en

Independent variations of CH4 ...... on over the past 160,000 years

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Independent variations of CH4 ...... on over the past 160,000 years

@en

Independent variations of CH4 ...... on over the past 160,000 years

@nl

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Nature Geoscience

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Independent variations of CH4 ...... on over the past 160,000 years

@en

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Heinrich Miller

http://www.w3.org/2001/XMLSchema#string

Lars Möller

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Michael Bock

http://www.w3.org/2001/XMLSchema#string

Renato Spahni

http://www.w3.org/2001/XMLSchema#string

Todd Sowers

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P2860

Wildfire responses to abrupt climate change in North America

Thermokarst lakes as a source of atmospheric CH4 during the last deglaciation

Eight glacial cycles from an Antarctic ice core

Late Quaternary atmospheric CH4 isotope record suggests marine clathrates are stable

Wet phases in the Sahara/Sahel region and human migration patterns in North Africa

Carbon isotopic evidence for methane hydrate instability during quaternary interstadials

Orbital and millennial-scale features of atmospheric CH4 over the past 800,000 years.

Wet periods in northeastern Brazil over the past 210 kyr linked to distant climate anomalies.

Atmospheric CO2 and climate on millennial time scales during the last glacial period.

Hydrogen isotopes preclude marine hydrate CH4 emissions at the onset of Dansgaard-Oeschger events.

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885-890

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scholarly article

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10.1038/NGEO1922

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10

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6

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Hubertus Fischer

Melanie Behrens

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2013-08-25T00:00:00Z

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1033758210

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